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Death Valley National Park, California. Furnace Creek Formation at the north end of the Black Mountains. View is southwest and west of Zabriskie Point, an overlook by Highway 190 about 3 miles up Furnace Creek Wash from Furnace Creek Inn. The base of the Furnace Creek Formation is at the topographic break between the badlands and the rougher, higher ground in the distance on the left. Light-colored playa beds about 2,500 feet thick extend to the base of a conglomerate which forms the dark cliff at the right. The beds are dipping to the right (north) into the Texas Spring Syncline. The center of the photograph looks west across Death Valley to the Panamint Range at Aguereberry Point; Tucki Mountain on the right....
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Death Valley National Park, California. Furnace Creek Formation at the north end of the Black Mountains. View is southwest and west of Zabriskie Point, an overlook by Highway 190 about 3 miles up Furnace Creek Wash from Furnace Creek Inn. The base of the Furnace Creek Formation is at the topographic break between the badlands and the rougher, higher ground in the distance on the left. Light-colored playa beds about 2,500 feet thick extend to the base of a conglomerate which forms the dark cliff at the right. The beds are dipping to the right (north) into the Texas Spring Syncline. The center of the photograph looks west across Death Valley to the Panamint Range at Aguereberry Point; Tucki Mountain on the right....
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Death Valley National Park, California. Fractured cobble conglomerate in the Titus Canyon(?) Formation of Stock and Bode (1935). The fractures extend through the cobbles, and some cross from one cobble to another. They are oriented at right angles to the bedding, which approximately parallels the elongation of the cobbles. Displacements along the fractures are mostly less than a quarter of an inch. Circa 1960. Figure 41, U.S. Geological Survey Professional Paper 494-A.
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Death Valley National Park, California. Thin-bedded middle member of the Bonanza King Formation on the north side of Trail Canyon. View is north. This member, about 600 feet thick, forms a distinctive unit separating massive thick-bedded dolomite comprising the upper and lower members of the formation. Circa 1960. Figure 22, U.S. Geological Survey Professional Paper 494-A.
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Death Valley National Park, California. Ovaloid brachiopods may be found in light tan, shaly and sandy beds that occur near the middle of the Bonanza King Formation. With the brachiopods are fragments of trilobites. Circa 1960.
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Township 22 north, Range 1 west, northeast 1/4 Section 35, view north. Mesaverde formation nearly vertical (sandstone beds make light ridges) and truncated by erosion surface sloping west from Nacimiento Mountains. Sandoval County, New Mexico. 1933.
    map background search result map search result map Thin-bedded middle member of the Bonanza King Formation on the north side of Trail Canyon. Death Valley National Park, California. Circa 1960. Fractured cobble conglomerate in the Titus Canyon(?) Formation of Stock and Bode (1935). Death Valley National Park, California. Circa 1960. Ovaloid brachiopods may be found in light tan, shaly and sandy beds that occur near the middle of the Bonanza King Formation. Death Valley National Park, California. Circa 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. Circa 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. Circa 1960. Mesaverde formation nearly vertical (sandstone beds make light ridges) and truncated by erosion surface sloping west from Nacimiento Mountains. Sandoval County, New Mexico. 1933. Mesaverde formation nearly vertical (sandstone beds make light ridges) and truncated by erosion surface sloping west from Nacimiento Mountains. Sandoval County, New Mexico. 1933. Thin-bedded middle member of the Bonanza King Formation on the north side of Trail Canyon. Death Valley National Park, California. Circa 1960. Fractured cobble conglomerate in the Titus Canyon(?) Formation of Stock and Bode (1935). Death Valley National Park, California. Circa 1960. Ovaloid brachiopods may be found in light tan, shaly and sandy beds that occur near the middle of the Bonanza King Formation. Death Valley National Park, California. Circa 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. Circa 1960. Furnace Creek Formation at the north end of the Black Mountains. Death Valley National Park, California. Circa 1960.